Campi Flegrei Mar Sicilia
Campi Flegrei del Mar di Sicilia
화산대지 · Italy · 8m (해저)

- 화산 유형
- 화산대지
- 국가
- Italy
- 지역
- European Volcanic Regions / Sicily Volcanic Province
- 해발
- 8m (해저)
- 좌표
- 37.100, 12.700
- 마지막 분화
- 1867년
- 판구조 환경
- Rift zone / Continental crust (> 25 km)
- 화산 지형
- Cluster
- 주요 암석
- Trachybasalt / Tephrite Basanite
지질학적 요약
Campi Flegrei del Mar di Sicilia (Phlegraean Fields of the Sicily Sea) is composed of a group of submarine volcanoes SW of Sicily. The volcanoes were constructed within a submarine depression about 1 km deep in the Strait of Sicily between the SW coast of Sicily and the NE tip of Tunisia, forming submarine banks that are capped by cones that rise to near sea level. Submarine eruptions were reported at the Giulia-Ferdinandeo and Pinne banks during the first Punic war (264-241 BCE), and from the 17th to 20th centuries, sometimes producing ephemeral islands. The 1831 eruption at Ferdinandea (also known as Graham in English or Giulia/Julia in French) produced an ephemeral island that was promptly claimed by the navies of France, Britain, Spain, and Italy.
Wikipedia 요약
영어 요약Campi Flegrei del Mar di Sicilia is a field of submarine volcanoes located south-west of Sicily. It includes the vent of Ferdinandea, otherwise known as Graham Island, which erupted and emerged above sea level in 1831, and encompasses a larger volcano known as Empedocles. The last recorded eruption was in 1867, from a vent named Pinne. There was mild seismic unrest at Ferdinandea in 2000–2002. At its highest, Campi Flegrei comes to 8 meters below sea level.
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분화 이력
상세 타임라인
- 1911년VEI 1지질학적 추정1911-09-30 ~ 진행 중Pinne
- 1867년VEI 0관측 기록1867 ~ 진행 중Pinne
- 1863년VEI 2관측 기록1863-08-12 ~ 진행 중Giulia Ferdinandeo
- 1846년VEI 2관측 기록1846-10-04 ~ 1846-10-05Pinne
- 1831년VEI 3관측 기록1831-06-28 ~ 1831-08-11Giulia Ferdinandeo (Graham Island)
- 1701년VEI 2지질학적 추정1701 ~ 진행 중Giulia Ferdinandeo
- 1632년VEI 0관측 기록1632 ~ 진행 중Giulia Ferdinandeo
- 기원전 253년 (±12년)VEI ?관측 기록BCE 253 ~ 진행 중
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